The interactions between CO2 and reservoirs under low-temperature
cooling conditions can change the pore throat characteristics of the
corresponding rocks. In this work, the interaction mechanisms between
liquid CO2 cooling and pore throat systems of shale were
researched using nuclear magnetic resonance (NMR) technology. Five
typical shale core samples were selected and subjected to liquid CO2 cooling experiments under different conditions. Furthermore,
the change ranges of the pores were quantitatively calculated based
on the NMR T
2 spectra. The results indicate
that the overall pore throat system of the shale changes after liquid
CO2 cooling. The factors influencing the degree of change
are the pore throat structure, liquid CO2 cooling temperature,
and cooling time. The degree of change for different pores are related
to the relative contents of the pores in the initial state. When the
liquid CO2 cooling experiments comprise one, two, and three
iterations, the average overall increase in the NMR T
2 spectrum are 2.56, 5.81, and 8.97%, respectively, and
the average increase of the smaller pores are 0.77, 0.92, and 1.84%,
respectively. The overall pore throat system changes greatly with
an increase in the liquid CO2 cooling times, and the degree
of change in the smaller pores increases. When the liquid CO2 cooling temperature of core sample A2 ranges from −30 to
−20 °C, the increase in the T
2 spectrum is between 3.57 and 2.20%. When the liquid CO2 cooling temperature of core sample B2 is increased from −30
to −20 to −10 °C, the increases in the T
2 spectrum are 2.97, 2.90, and 2.79%, respectively.
As the temperature of the liquid CO2 increases, the change
in the overall pore throat system is weakened. The smaller pores change
more obviously after liquid CO2 cooling within a certain
low-temperature range. The degree of change of the larger pores is
less affected by temperature.